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Planetary News: Cassini-Huygens (2005)

New RADAR Images of Titan:

The Features Are Getting More Familiar, But Aren't Getting Less Mysterious

By Emily Lakdawalla
November 2, 2005

In a much-anticipated encounter, Cassini zoomed within 1,353 kilometers (841 miles) of Titan last Friday and achieved the first RADAR imaging of the Huygens landing site.  Have all of the mysteries of the Huygens landing site been answered?  In a word, no.  "It's not easy!" remarked Rosaly Lopes, a member of the Cassini RADAR team.  "We didn't really expect it to be."

The following images show all of the available views of the Huygens landing site from different Cassini and Huygens instruments.  First, for comparison, here is the best available view that was put together from dozens of individual frames from Huygens' Descent Imager / Spectral Radiometer (DISR):

Large surface mosaic of Titan
Large surface mosaic of Titan
This mosaic was stitched by amateur image processor René Pascal from the Huygens DISR data. The mosaic is mostly composed of Medium Resolution Imager data, supplemented with some High Resolution Imager and some Side Looking Imager data. Credit: ESA / NASA / JPL / University of Arizona / René Pascal

The fortunate fact that Huygens appeared to descend across the border between bright regions and dark regions is helping match the DISR panorama to images from the Cassini orbiter.  But that is pretty much where the good luck ended for those interested in locating the Huygens landing site on the orbiter's images.  Titan’s cloud deck proved to be much lower than the Huygens team expected.  As a result, their views from higher altitudes -- which would have spanned a larger area than the lower-altitude views -- could not see the surface.  Furthermore, the thick haze, turbulent atmosphere, and the unexpected backwards rotation of Huygens during its descent stymied its Sun sensor, so the compass orientation of the Huygens images is only approximately known, making the match even more difficult.

Predicted location of the Huygens landing site
To create this map, data from two other maps were merged to remove other map markings, and some gaps where both maps had annotations were filled in by airbrushing. Credit: NASA / JPL / Space Science Institute / Emily Lakdawalla

Huygens’ final mosaics contain beautiful detail, but the images are in fact so detailed and of such a small area that they can’t be matched precisely to the much fuzzier orbiter views.  The map at right is the best published view from the Cassini Imaging Science Subsystem (ISS).  The yellow dot on the map represents the guess at where Huygens would land based on predictions of Huygens' descent path prior to the Huygens mission on January 14.

Guess at the location of the Huygens landing site
Credit: NASA / JPL / University of Arizona / USGS

This map is the best published view available from the Cassini Visual and Infrared Mapping Spectrometer (VIMS).  The red circle on the map represents the guess at the landing site location after the Huygens landing based on comparison of the VIMS and DISR images.

Huygens' landing site as seen by Cassini RADAR
Credit: NASA / JPL

Finally, this is the Synthetic Aperture RADAR (SAR) image of the Huygens landing site.  The yellow outline and magenta cross mark the best guess of the RADAR team at the location of the Huygens DISR images.  But Lopes was cautious about the lines drawn on the map, saying "the location of the landing site is more uncertain than the map implies, so this is preliminary.  It may be revised in the future."

All of the maps and images above are shown at different scales, making comparisons difficult.  Here are comparison images showing the available image data at the same scale and covering approximately the same areas.  Each image represents an area 500 kilometers (310 miles) square.

Huygens' landing site: ISS Huygens' landing site: VIMS
Huygens' landing site: ISS
Credit: NASA / JPL / Space Science Institute
Huygens' landing site: VIMS
Credit: NASA / JPL / University of Arizona /
USGS
Huygens' landing site: colorized imagery Huygens' landing site: RADAR
Huygens' landing site: colorized composite
of data from ISS and VIMS

Credit: NASA / JPL / University of Arizona /
Space Science Institute
Huygens' landing site: RADAR
Credit: NASA / JPL

A first impression, comparing the SAR image to the VIMS and ISS images, shows that the patterns of brightness and darkness, also known as "albedo," in the VIMS and ISS images do not match the broad variations in the SAR images.  "What's light and dark in RADAR is not necessarily what's light and dark in visible wavelengths," Lopes pointed out.  "This makes it kind of difficult to pinpoint the exact location of Huygens."

Titan's diverse surface as seen by Cassini RADAR
A wide variety of terrains is visible in this RADAR image. Brightly reflective regions are probably high-standing topographic features. Darker areas are covered with the east-west oriented linear features that scientists refer to as "cat scratches." The darkest regions have a channel-like appearance and could once have contained -- or may still contain -- fluids. This picture covers an area about 300 by about 200 kilometers (180 by 120 miles) across. Source Credit: NASA / JPL
Cat scratches on Titan
In this image, the cat scratches appear to flow around brighter regions that are interpreted to be high-standing ridges. Credit: NASA / JPL
Possible ridges on Titan as seen in Cassini RADAR
Scientists interpret the bright, curving features to be topographically high ridges. Their linear shape suggests that they are tectonic in origin, meaning that they resulted from the deformation of Titan's crust, much as mountain ranges form on Earth. The image covers an area about 400 by 275 kilometers (250 by 170 miles) in size. Source Credit: NASA / JPL

However, closer investigation of the images reveals that there are a few clear correlations.  Large areas of the SAR image are covered with "cat scratches," east-west aligned sets of parallel, dark lines.  Cat scratches in SAR images broadly correlate with low albedo in the ISS and VIMS images.  In fact, everywhere the science team looked in the new SAR images, "we see lots of cat scratches, really lots of them," Lopes said.  "They are starting to look pretty common on Titan, but mostly at lower latitudes.  We still think that they are aeolian but there is still debate about that."

The team is yet lacking some data that would be useful in interpreting what the cat scratches are.  Cassini captures the data for SAR imagery by broadcasting a radio signal at Titan and listening for its echo; the effect is similar to seeing in the dark using a flashlight.  Almost all of the SAR swaths that Cassini has acquired to date were captured when Cassini was flying in an east-west direction across Titan.  As a result, nearly all of the SAR swaths are illuminated from the north or south.  Lopes is looking forward to a future SAR swath captured from a different illumination direction.  "We are wondering whether looking at the cat scratches from a different direction would help us constrain [their origin] better.  Because at the moment we are only seeing them perpendicular to the SAR.  They are east-west and we are looking north-south.  Maybe we wouldn't see them if we were looking in another direction."

The most exciting features Lopes saw in the new SAR swath were "long ridges that we think are tectonic.  We have not seen those before.  We can't tell how high they are, but we think they are ridges of hills.  In the SAR they look bright."  The ridges or hills seem to crop up out of smoother regions filled with cat scratches.  Lopes noted that the cat scratches appear to be diverted by these hills and flow around them, supporting both the notion that the hills are in fact topographic features and the theory that the cat scratches are aeolian and aligned with the motion of surface winds.

Unfortunately, it is not yet possible to be certain of the topography across areas seen in the SAR images, because Cassini cannot acquire SAR images and altimetric measurements simultaneously.  "As the mission goes on we'll begin to get altimetry over the SAR, and that's when it will get really interesting," Lopes said.  But what the RADAR team is really waiting for is the opportunity to see two regions on Titan at different RADAR "look angles."  This will only happen when two SAR swaths overlap.  The first opportunity to get overlapping SAR coverage does not occur for another year, during the Titan-20 ("T20") flyby on October 26, 2006.  Cassini mission planners have not yet decided whether to take advantage of this opportunity.

Large impact basin on Titan
Large impact basin on Titan
A large structure seen in RADAR images from Cassini's February 15, 2005 Titan flyby is likely a multi-ringed impact basin. Its rim has been heavily modified by erosion into gullies and channels. The basin is being referred to as "Circus Maximus" by the science team. The entire basin is about 440 kilometers (273 miles) across, or nearly ten percent the diameter of Titan. Source Credit: NASA / JPL

"We planned the T20 flyby two ways," Lopes said.  "It's a very good flyby for a number of instruments, but of course we can't acquire optical remote sensing and RADAR data at the same time, so we will have to chose one or the other." The decision will be made in January of 2006.  "We are hoping that the project science group will decide in our favor.  If we get it, we will have a new SAR swath that will cross over that big impact crater we saw in T3," the Titan flyby that occurred on February 15, 2005. 

Each Titan flyby delivers loads of new data, but rather than answering questions the data always seems to whet our appetites even more.  Fortunately, this was only the ninth of 45 planned flybys.  The next Titan flyby occurs on December 26.